Beyond Plate Tectonics: Looking at Plate Deformation with Space Geodesy
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Geodetic Surveying, Earth Modeling, and the New Geodetic Datum of 2022
Geodetic Surveying, Earth Modeling, and the New Geodetic Datum of 2022 PDH330 3 Hours PDH Academy PO Box 449 Pewaukee, WI 53072 (888) 564-9098 www.pdhacademy.com [email protected] Geodetic Surveying Final Exam 1. Who established the U.S. Coast and Geodetic Survey? A) Thomas Jefferson B) Benjamin Franklin C) George Washington D) Abraham Lincoln 2. Flattening is calculated from what? A) Equipotential surface B) Geoid C) Earth’s circumference D) The semi major and Semi minor axis 3. A Reference Frame is based off how many dimensions? A) two B) one C) four D) three 4. Who published “A Treatise on Fluxions”? A) Einstein B) MacLaurin C) Newton D) DaVinci 5. The interior angles of an equilateral planar triangle adds up to how many degrees? A) 360 B) 270 C) 180 D) 90 6. What group started xDeflec? A) NGS B) CGS C) DoD D) ITRF 7. When will NSRS adopt the new time-based system? A) 2022 B) 2020 C) Unknown due to delays D) 2021 8. Did the State Plane Coordinate System of 1927 have more zones than the State Plane Coordinate System of 1983? A) No B) Yes C) They had the same D) The State Plane Coordinate System of 1927 did not have zones 9. A new element to the State Plane Coordinate System of 2022 is: A) The addition of Low Distortion Projections B) Adjoining tectonic plates C) Airborne gravity collection D) None of the above 10. The model GRAV-D (Gravity for Redefinition of the American Vertical Datum) created will replace _____________ and constitute the new vertical height system of the United States A) Decimal degrees B) Minutes C) NAVD 88 D) All of the above Introduction to Geodetic Surveying The early curiosity of man has driven itself to learn more about the vastness of our planet and the universe. -
Geodesy in the 21St Century
Eos, Vol. 90, No. 18, 5 May 2009 VOLUME 90 NUMBER 18 5 MAY 2009 EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION PAGES 153–164 geophysical discoveries, the basic under- Geodesy in the 21st Century standing of earthquake mechanics known as the “elastic rebound theory” [Reid, 1910], PAGES 153–155 Geodesy and the Space Era was established by analyzing geodetic mea- surements before and after the 1906 San From flat Earth, to round Earth, to a rough Geodesy, like many scientific fields, is Francisco earthquakes. and oblate Earth, people’s understanding of technology driven. Over the centuries, it In 1957, the Soviet Union launched the the shape of our planet and its landscapes has developed as an engineering discipline artificial satellite Sputnik, ushering the world has changed dramatically over the course because of its practical applications. By the into the space era. During the first 5 decades of history. These advances in geodesy— early 1900s, scientists and cartographers of the space era, space geodetic technolo- the study of Earth’s size, shape, orientation, began to use triangulation and leveling mea- gies developed rapidly. The idea behind and gravitational field, and the variations surements to record surface deformation space geodetic measurements is simple: Dis- of these quantities over time—developed associated with earthquakes and volcanoes. tance or phase measurements conducted because of humans’ curiosity about the For example, one of the most important between Earth’s surface and objects in Earth and because of geodesy’s application to navigation, surveying, and mapping, all of which were very practical areas that ben- efited society. -
NASA Space Geodesy Program: Catalogue of Site Information
NASA Technical Memorandum 4482 NASA Space Geodesy Program: Catalogue of Site Information M. A. Bryant and C. E. Noll March 1993 N93-2137_ (NASA-TM-4482) NASA SPACE GEODESY PROGRAM: CATALOGUE OF SITE INFORMATION (NASA) 688 p Unclas Hl146 0154175 v ,,_r NASA Technical Memorandum 4482 NASA Space Geodesy Program: Catalogue of Site Information M. A. Bryant McDonnell Douglas A erospace Seabro'ok, Maryland C. E. Noll NASA Goddard Space Flight Center Greenbelt, Maryland National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland 20771 1993 . _= _qum_ Table of Contents Introduction .......................................... ..... ix Map of Geodetic Sites - Global ................................... xi Map of Geodetic Sites - Europe .................................. xii Map of Geodetic Sites - Japan .................................. xiii Map of Geodetic Sites - North America ............................. xiv Map of Geodetic Sites - Western United States ......................... xv Table of Sites Listed by Monument Number .......................... xvi Acronyms ............................................... xxvi Subscription Application ..................................... xxxii Site Information ............................................. Site Name Site Number Page # ALGONQUIN 67 ............................ 1 AMERICAN SAMOA 91 ............................ 5 ANKARA 678 ............................ 9 AREQUIPA 98 ............................ 10 ASKITES 674 ........................... , 15 AUSTIN 400 ........................... -
Space Geodesy and Satellite Laser Ranging
Space Geodesy and Satellite Laser Ranging Michael Pearlman* Harvard-Smithsonian Center for Astrophysics Cambridge, MA USA *with a very extensive use of charts and inputs provided by many other people Causes for Crustal Motions and Variations in Earth Orientation Dynamics of crust and mantle Ocean Loading Volcanoes Post Glacial Rebound Plate Tectonics Atmospheric Loading Mantle Convection Core/Mantle Dynamics Mass transport phenomena in the upper layers of the Earth Temporal and spatial resolution of mass transport phenomena secular / decadal post -glacial glaciers polar ice post-glacial reboundrebound ocean mass flux interanaual atmosphere seasonal timetime scale scale sub --seasonal hydrology: surface and ground water, snow, ice diurnal semidiurnal coastal tides solid earth and ocean tides 1km 10km 100km 1000km 10000km resolution Temporal and spatial resolution of oceanographic features 10000J10000 y bathymetric global 1000J1000 y structures warming 100100J y basin scale variability 1010J y El Nino Rossby- 11J y waves seasonal cycle eddies timetime scale scale 11M m mesoscale and and shorter scale fronts physical- barotropic 11W w biological variability interaction Coastal upwelling 11T d surface tides internal waves internal tides and inertial motions 11h h 10m 100m 1km 10km 100km 1000km 10000km 100000km resolution Continental hydrology Ice mass balance and sea level Satellite gravity and altimeter mission products help determine mass transport and mass distribution in a multi-disciplinary environment Gravity field missions Oceanic -
Geodetic Position Computations
GEODETIC POSITION COMPUTATIONS E. J. KRAKIWSKY D. B. THOMSON February 1974 TECHNICALLECTURE NOTES REPORT NO.NO. 21739 PREFACE In order to make our extensive series of lecture notes more readily available, we have scanned the old master copies and produced electronic versions in Portable Document Format. The quality of the images varies depending on the quality of the originals. The images have not been converted to searchable text. GEODETIC POSITION COMPUTATIONS E.J. Krakiwsky D.B. Thomson Department of Geodesy and Geomatics Engineering University of New Brunswick P.O. Box 4400 Fredericton. N .B. Canada E3B5A3 February 197 4 Latest Reprinting December 1995 PREFACE The purpose of these notes is to give the theory and use of some methods of computing the geodetic positions of points on a reference ellipsoid and on the terrain. Justification for the first three sections o{ these lecture notes, which are concerned with the classical problem of "cCDputation of geodetic positions on the surface of an ellipsoid" is not easy to come by. It can onl.y be stated that the attempt has been to produce a self contained package , cont8.i.ning the complete development of same representative methods that exist in the literature. The last section is an introduction to three dimensional computation methods , and is offered as an alternative to the classical approach. Several problems, and their respective solutions, are presented. The approach t~en herein is to perform complete derivations, thus stqing awrq f'rcm the practice of giving a list of for11111lae to use in the solution of' a problem. -
GPS and the Search for Axions
GPS and the Search for Axions A. Nicolaidis1 Theoretical Physics Department Aristotle University of Thessaloniki, Greece Abstract: GPS, an excellent tool for geodesy, may serve also particle physics. In the presence of Earth’s magnetic field, a GPS photon may be transformed into an axion. The proposed experimental setup involves the transmission of a GPS signal from a satellite to another satellite, both in low orbit around the Earth. To increase the accuracy of the experiment, we evaluate the influence of Earth’s gravitational field on the whole quantum phenomenon. There is a significant advantage in our proposal. While the geomagnetic field B is low, the magnetized length L is very large, resulting into a scale (BL)2 orders of magnitude higher than existing or proposed reaches. The transformation of the GPS photons into axion particles will result in a dimming of the photons and even to a “light shining through the Earth” phenomenon. 1 Email: [email protected] 1 Introduction Quantum Chromodynamics (QCD) describes the strong interactions among quarks and gluons and offers definite predictions at the high energy-perturbative domain. At low energies the non-linear nature of the theory introduces a non-trivial vacuum which violates the CP symmetry. The CP violating term is parameterized by θ and experimental bounds indicate that θ ≤ 10–10. The smallness of θ is known as the strong CP problem. An elegant solution has been offered by Peccei – Quinn [1]. A global U(1)PQ symmetry is introduced, the spontaneous breaking of which provides the cancellation of the θ – term. As a byproduct, we obtain the axion field, the Nambu-Goldstone boson of the broken U(1)PQ symmetry. -
Space Geodesy and Earth System (SGES 2012) Aug 18-25, 2012, Shanghai, China
International Symposium & Summer School on Space Geodesy and Earth System (SGES 2012) Aug 18-25, 2012, Shanghai, China http://www.shao.ac.cn/meetings; http://www.shao.ac.cn/schools Venue: 3rd floor of Astronomical Building Shanghai Astronomical Observatory, Chinese Academy of Sciences International Symposium on Space Geodesy and Earth Sytem (SGES2012) August 18-21, 2011, Shanghai, China http://www.shao.ac.cn/meetings Contact Information: Email: [email protected]; [email protected] Emergency Phone: 13167075822 Police: 110; Ambulance: 120 Venue: 3rd floor, Astronomical Building Shanghai Astronomical Observatory, Chinese Academy of Sciences 80 Nandan Road, Shanghai 200030, China Available WIFI at the workshop with the password at conference hall doors Sponsors • International Association of Geodesy (IAG) Commission 1, 3, 4 • International Association of Geodesy Sub-Commission 2.6 • Asia-Pacific Space Geodynamics Program (APSG) • Global Geodetic Observing System (GGOS) • Shanghai Astronomical Observatory (SHAO), CAS 1 Scientific Organizing Committee (SOC) • Zuheir Altamimi (IGN, France) • Jeff T. Freymueller (Uni. Alaska, USA) • Richard S. Gross (JPL, NASA, USA) • Manabu Hashimoto (Kyoto Uni., Japan) • Shuanggen Jin (SHAO, CAS, China) (Chair) • Roland Klees (TUDelft, Netherlands) • Christopher Kotsakis (AUTH, Greece) • Michael Pearlman (Harvard-CFA, USA) • Wenke Sun (Grad. Uni. of CAS, China) • Harald Schuh (TU-Vienna, Austria) • Tonie van Dam (Univ. Luxembourg) • Jens Wickert (GFZ Potsdam, Germany) • Shimon Wdowinski (Univ. Miami, USA) Local -
VLBI, GNSS, and DORIS Systems
The NASA Space Geodesy Project Frank Lemoine & Chopo Ma April 5, 2012 Background • Space geodetic systems provide the measurements that are needed to define and maintain an International Terrestrial Reference Field (ITRF) • The ITRF is realized through a combination of observations from globally distributed SLR, VLBI, GNSS, and DORIS systems • NASA contributes SLR, VLBI and GNSS systems to the global network, and has since the Crustal Dynamics Project in the 1980’s • But: the NASA systems are mostly “legacy” systems VLBI SLR GPS DORIS Doppler Orbitography and Radio Positioning Very Long Baseline Satellite Laser Ranging Global Positioning System Integrated by Satellite Interferometry Space Geodesy Project – 04/05/2012 2 ITRF Requirements • Requirements for the ITRF have increased dramatically since the 1980’s – Most stringent requirement comes from sea level studies: “accuracy of 1 mm, and stability at 0.1 mm/yr” – This is a factor 10-20 beyond current capability • Simulations show the required ITRF is best realized from a combination solution using data from a global network of ~30 integrated stations having all available techniques with next generation measurement capability – The current network cannot meet this requirement, even if it could be maintained over time (which it cannot) • The core NASA network is deteriorating and inadequate Space Geodesy Project – 04/05/2012 3 Geodetic Precision and Time Scale http://dels.nas.edu/Report/Precise-Geodetic-Infrastructure-National-Requirements/12954 Space Geodesy Project – 04/05/2012 4 NRC Recommendations • Deploy the next generation of automated high-repetition rate SLR tracking systems at the four current U.S. tracking sites in Hawaii, California, Texas, and Maryland; • Install the next-generation VLBI systems at the four U.S. -
JHR Final Report Template
TRANSFORMING NAD 27 AND NAD 83 POSITIONS: MAKING LEGACY MAPPING AND SURVEYS GPS COMPATIBLE June 2015 Thomas H. Meyer Robert Baron JHR 15-327 Project 12-01 This research was sponsored by the Joint Highway Research Advisory Council (JHRAC) of the University of Connecticut and the Connecticut Department of Transportation and was performed through the Connecticut Transportation Institute of the University of Connecticut. The contents of this report reflect the views of the authors who are responsible for the facts and accuracy of the data presented herein. The contents do not necessarily reflect the official views or policies of the University of Connecticut or the Connecticut Department of Transportation. This report does not constitute a standard, specification, or regulation. i Technical Report Documentation Page 1. Report No. 2. Government Accession No. 3. Recipient’s Catalog No. JHR 15-327 N/A 4. Title and Subtitle 5. Report Date Transforming NAD 27 And NAD 83 Positions: Making June 2015 Legacy Mapping And Surveys GPS Compatible 6. Performing Organization Code CCTRP 12-01 7. Author(s) 8. Performing Organization Report No. Thomas H. Meyer, Robert Baron JHR 15-327 9. Performing Organization Name and Address 10. Work Unit No. (TRAIS) University of Connecticut N/A Connecticut Transportation Institute 11. Contract or Grant No. Storrs, CT 06269-5202 N/A 12. Sponsoring Agency Name and Address 13. Type of Report and Period Covered Connecticut Department of Transportation Final 2800 Berlin Turnpike 14. Sponsoring Agency Code Newington, CT 06131-7546 CCTRP 12-01 15. Supplementary Notes This study was conducted under the Connecticut Cooperative Transportation Research Program (CCTRP, http://www.cti.uconn.edu/cctrp/). -
Coordinate Systems in Geodesy
COORDINATE SYSTEMS IN GEODESY E. J. KRAKIWSKY D. E. WELLS May 1971 TECHNICALLECTURE NOTES REPORT NO.NO. 21716 COORDINATE SYSTElVIS IN GEODESY E.J. Krakiwsky D.E. \Vells Department of Geodesy and Geomatics Engineering University of New Brunswick P.O. Box 4400 Fredericton, N .B. Canada E3B 5A3 May 1971 Latest Reprinting January 1998 PREFACE In order to make our extensive series of lecture notes more readily available, we have scanned the old master copies and produced electronic versions in Portable Document Format. The quality of the images varies depending on the quality of the originals. The images have not been converted to searchable text. TABLE OF CONTENTS page LIST OF ILLUSTRATIONS iv LIST OF TABLES . vi l. INTRODUCTION l 1.1 Poles~ Planes and -~es 4 1.2 Universal and Sidereal Time 6 1.3 Coordinate Systems in Geodesy . 7 2. TERRESTRIAL COORDINATE SYSTEMS 9 2.1 Terrestrial Geocentric Systems • . 9 2.1.1 Polar Motion and Irregular Rotation of the Earth • . • • . • • • • . 10 2.1.2 Average and Instantaneous Terrestrial Systems • 12 2.1. 3 Geodetic Systems • • • • • • • • • • . 1 17 2.2 Relationship between Cartesian and Curvilinear Coordinates • • • • • • • . • • 19 2.2.1 Cartesian and Curvilinear Coordinates of a Point on the Reference Ellipsoid • • • • • 19 2.2.2 The Position Vector in Terms of the Geodetic Latitude • • • • • • • • • • • • • • • • • • • 22 2.2.3 Th~ Position Vector in Terms of the Geocentric and Reduced Latitudes . • • • • • • • • • • • 27 2.2.4 Relationships between Geodetic, Geocentric and Reduced Latitudes • . • • • • • • • • • • 28 2.2.5 The Position Vector of a Point Above the Reference Ellipsoid . • • . • • • • • • . .• 28 2.2.6 Transformation from Average Terrestrial Cartesian to Geodetic Coordinates • 31 2.3 Geodetic Datums 33 2.3.1 Datum Position Parameters . -
Infoag Conference NSRS Modernization 2022 New Datums Scott Lokken National Geodetic Survey, NOAA Mid Atlantic Regional Geodetic Advisor July 24, 2019
InfoAg Conference NSRS Modernization 2022 New Datums Scott Lokken National Geodetic Survey, NOAA Mid Atlantic Regional Geodetic Advisor July 24, 2019 July 24, 2019 1 NGS Regional Advisors • Geodesist • 31 Years with NGS • GIS Certified • Farm Kid from SE N.D. July 24, 2019 2 National Spatial Reference System (NSRS) NGS Mission: To define, maintain & provide access to the National Spatial Reference System (NSRS) to meet our Nation’s economic, social & environmental needs Consistent National Coordinate System • Latitude/Northing • Longitude/Easting • Height • Scale • Gravity • Orientation and how these values change with time. New Reference Systems Planned for 2022 • Replace NAD83 with a geocentric reference frame • GNSS based • Replace NAVD88 with a gravity based geoid • Replace: bluebooking, database, State Plane Coordinates July 24, 2019 • improve toolkit, surveying methodologies. 4 What matters to you? Required Accuracy vs Precision determines how the new datums will impact you. Low Precision HIgh Precision Low Precision High Precision Low Accuracy Low Accuracy High Accuracy High Accuracy July 24, 2019 5 Different times, different accuracy 2019 1981 July 24, 2019 6 Bottom Line, Up Front • If you do geospatial work in the USA… • and you work in the National Spatial Reference System.. • every product you’ve ever made… – every survey… – every map… – every lidar point cloud… – every image… – every DEM… – WILL have the wrong coordinates on it in 3 years. Let’s talk about what this means, why it is happening, and how it will affect things -
Geodesy: Trends and Prospects
Geodesy: Trends and Prospects Practktll and Scientific Values of Geodesy 25 clearly observable with the new long-baseline interferom We recommend that the United States support three long etry (LBI) and laser-ranging techniques. For example, the baseline-radio-interferometry stations and approximately 1960 Chilean earthquake (magnitude 8.3) has been calcu six laser ranging stations at fvced locations as part ofa new lated (Smith, 1977) to give a change in polar motion corre international service for determining UT and polar motion sponding to a 65-crn offset in the axis about which the pole on a continuing basis with suff~eient accuracy to meet cur moves, if the coseismic fault plane motion derived by Kana rent geodynamics needs. rnori and Cipar (1974) is used, and a possible additional 87 -ern offset due to the preseismic motion for which they The reasons for recommending support for these particu have presented evidence. lar numbers of stations are discussed in Section 4.2. It Seismologists generally believe that the "seismic mo should be noted that most of these stations also will fulfill ment" corresponding to the coseismic motion can be de other important scientific or applied objectives and that a rived accurately from observed long-period seismic-wave number of them are already available or will be soon. amplitudes. However, motions occurring over periods of minutes, days, or even several months before and after the quake are difficult to determine in other ways. Thus 3.3 OCEAN DYNAMICS changes in polar motion over a period of several months around the time of the quake can give a check on the total The geoid is considered to be the equipotential surface that fault displacement, which complements the information would enclose the ocean waters if all external forces were available from resurveys of the surface area surrounding the removed and the waters were to become still.